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Analytical method: XRF

TechniqueXRF
MaterialWHOLE ROCK
Mineralnone
InstitutionUNIVERSITY OF EDINBURGH, DEPARTMENT OF GEOLOGY AND GEOPHYSICS, EDINBURGH, EH9 3JW, UK
ReferenceKempton, P D; Fitton, J G; Hawkesworth, C J; Ormerod, D S (1991) Isotopic and trace element constraints on the composition and evolution of the lithosphere beneath the Southwestern United States. Journal of Geophysical Research, B, Solid Earth and Planets. 96; 8, Pages 13,713-13,735. 1991.

Samples analysed with this method

CA_4, D_12, NV_7, NM_39, NM_33, NM_30, AZ_95, U_73_A, ESC_1, Pan_26, Pan_27, SG_19, UT_5, UT_6, UT_7, UT_16, WAH_66, Zion_2, Zion_20, Zion_21, Zion_58, Zion_70, AZ_3, AZ_4, AZ_100, AZ_17, AZ_18, AZ_42, AZ_48, NM_2, NM_49, NM_51, NM_52, NM_56, NM_59, AZ_33, AZ_38, AZ_21, AZ_69, AZ_1, AZ_60, AZ_65, AZ_101, NM_61